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- Assessing the Record and Causes of Late Triassic Extinctions
- Early and Middle Triassic Trends in Diversity, Evenness
- The Ammonoid Recovery After the End−Permian Mass Extinction: Evidence from the Iran−Transcaucasia Area, Siberia, Primorye, and Kazakhstan
- Dating the Origin of Dinosaurs Hans-Dieter Suesa,1
- GEOLOGIC TIME SCALE V
- The Latitudinal Diversity Gradient of Tetrapods Across the Permo-Triassic Mass Extinction and Recovery Interval
- Paper Number: 4000 Cycle-Calibrated Magnetostratigraphy and Time Scales for the Early and Early- Late Triassic Zhang, Y.1, Li, M.2, 3, Ogg, J
- Albertiana 42 49 NOTE on the CONODONTS from the INDUAN-OLENEKIAN BOUNDARY
- No Mass Extinction for Land Plants at the Permian–Triassic Transition
- 2009 Geologic Time Scale Cenozoic Mesozoic Paleozoic Precambrian Magnetic Magnetic Bdy
- Latest Permian to Middle Triassic Cyclo-Magnetostratigraphy from The
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- 239138 Ladjavardi 1 Year 2015.Pdf (5.673Mb)
- Chronological Stratigraphy (Roger Burkhalter)
- Triassic Eustatic Variations Reexamined
- Lower Triassic)
- Geologic Time Scale
- IMPACT of the LATE TRIASSIC MASS EXTINCTION on FUNCTIONAL DIVERSITY and COMPOSITION of MARINE ECOSYSTEMS by ALEXANDER M
- Towards a Definition of the Induan-Olenekian Boundary: the Potential of Eurygnathodus Costatus and Eurygnathodus Hamadai As Inde
- Upper Induan and Lower Olenekian Conodont Assemblages from the Lowest Part of the Bac Thuy Formation in the Ban Ru Area, Northeastern Vietnam
- Discovery of the Early Spathian (Late Olenekian, Early Triassic) Ammonoid Tirolites in the Hiraiso Formation, South Kitakami Belt, Northeast Japan
- The Global Boundary Stratotype Section and Point (GSSP) of the Carnian Stage (Late Triassic) at Prati Di Stuores/Stuores Wiesen Section (Southern Alps, NE Italy)
- Status of Divisions of the International Geologic Time Scale
- Marine Anoxia and Delayed Earth System Recovery After the End-Permian Extinction
- The Geological Society of America Geologic Time Scale 1888 2013
- Comparative Size Evolution of Marine Clades from the Late Permian Through Middle Triassic
- A New Protophyllocladoxylon Wood from the Induan (Lower Triassic) Jiucaiyuan Formation in the Turpan-Hami Basin, Southern Bogda